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increase - WordPress.com
increase - WordPress.com

... “Would the Queensland floods have occurred if humans were not warming the climate through greenhouse-gas emissions?” • Climate change will affect the overall number and strength of extreme weather events. • Two slightly easier and much more useful questions: “Will floods in Queensland become more fr ...
Carbon cycle
Carbon cycle

... Humans and Ecology: What are we doing, what should we do, what can we do, and does it matter? ...
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PDF sample

... becoming less certain. This is a paradox that has worried me for a while. Some people have used it to pour scorn on the scientists trying to come to grips with the consequences of our meddling with the climate—our planet’s life-support system. They suggest the uncertainty means we don’t need to worr ...
techvols_tv2_ch_7 - Port of Vancouver
techvols_tv2_ch_7 - Port of Vancouver

... According to published reports, average global sea level has risen at around 2 mm/year during the last century. Most recent studies have concluded that the sea level will rise at a faster rate than in the last century due to the effects of global warming. The Inter-Governmental Panel on Climate Chan ...
Hawaii`s Changing Climate - School of Ocean and Earth Science
Hawaii`s Changing Climate - School of Ocean and Earth Science

... [email protected] ...
Where Are You From? Why Are You Here? An African Perspective
Where Are You From? Why Are You Here? An African Perspective

... article Henry Stommel (1995) circulated in 1954, a few years after his pioneering paper that explains how the torque that easterly and westerly winds exert on the oceans—a rapidly rotating spherical shell of fluid—generates intense jets such as the Gulf Stream and the Kuroshio Current (Stommel 1948). ...
Queensland Climate Change Centre of Excellence (QCCCE)
Queensland Climate Change Centre of Excellence (QCCCE)

...  Simulation of historical & future climate using global coupled and uncoupled GCMs (C20C, Impact of LCLU on Australian climate, AR5)  Dynamical downscaling of data from the global climate models for Queensland region (both for climate change and seasonal forecasting)  Analysis of IPCC model datas ...
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420 Million years ago - Global Warming

... water vapor & albedo effects of reduced sulfates, snow, ice, and clouds. For clouds, 60% of the amount from AMO 2013 is used. Cloud changes are complex and explain part of warming to date. The effect of Arctic sea ice loss from Hudson (2011) is used: globally, 0.7 W / sq meter for total loss, during ...
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Slide 1

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2016 State of the Climate Report
2016 State of the Climate Report

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UnderStanding the UnFccc negotiationS a timeline oF the United

... Process to agree new treaty covering all countries was established at COP17 Durban in 2011. Governments have to disclose their targets and measures in March, and then conclude negotiations in Paris in December 2015, with treaty in force from 2020. The goal is a global climate agreement covering all ...
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IPRC News

... has the frequency of weather conditions, such as Kona Lows, that produce heavy rainfall events over Hawai‘i. These are the conclusions of IPRC’s Assistant Researcher Oliver Elison Timm, who has been studying the effects of climate change on rainfall, drought, and evapotranspiration across the Hawaii ...
climate change brief - Montana State University
climate change brief - Montana State University

... increased 1.1 0F / 100 years since 1900. Mean annual minimum temperatures, which indicate nighttime conditions, have increased more rapidly (1.5 0F/ 100 years) than mean annual maximum temperatures (0.7 0F/ 100 years), which indicate daytime conditions (Fig. 1). The GYE is subject to multiple-year p ...
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1 How do we know that climate change is happening?

... Back in the 1800s, a number of scientists were mucking about with gases in order to learn more about how the atmosphere worked. The French mathematician Joseph Fourier had realized in the 1820s that there must be something in the air that prevented the Sun’s heat from just bouncing off the Earth and ...
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Presented

... modest when amortized over thousands of units for many years to come. Q.2 Why the private companies would be interested to do that? It has a large business opportunity and huge profit potential. Currently, billions and hundreds of millions US dollars are spent each year in ocean/climate monitoring a ...
How is climate change affecting life on Earth?
How is climate change affecting life on Earth?

...  A1B: Rapid growth of technology and economies, but population grows slowly. There is less disparity between developing and developed countries.  A2: Economies grow but there is more disparity between developing and developed countries. Energy use is high and population is growing rapidly.  B1: D ...
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Introduction to Climate change Study Cell

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Introduction - San Jose State University
Introduction - San Jose State University

... Positive Feedbacks  Processes that accelerate a change – Note: Feedbacks cannot initiate change; they can only alter the pace of change ...
Slide 1 - University of Washington
Slide 1 - University of Washington

... Relatively small overall changes because effects of warming (decreased risks) and increased precipitation variability (increased risks) are in the opposite directions. ...
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2005 Exxon Foundation 990 vs Exxon Giving Report

... Under increasing scrutiny and pressure over the past two years from scientists, policy makers and the public, the company was forced to reveal that it had stopped funding a handful of organizations identified as part of the company’s denial campaign on global warming. In July 2006, ExxonMobil met wi ...
Introduction - San Jose State University
Introduction - San Jose State University

... Imagine the Earth was to warm for some reason (initiating mechanism or perturbation) A) Identify two positive feedbacks that would influence the earth’s climate and explain how each one works. B) Identify two negative feedbacks that would influence the earth’s climate and explain how each one works. ...
Systematic Observation Requirements for Space
Systematic Observation Requirements for Space

... Achieving an optimal balance of satellite and in-situ data  Ensuring data are stable enough to allow reliable detection of climate change –  20 GCOS climate monitoring principles (10 basic + 10 especially for space-based observations)  Making full use of all available data to achieve a costeffect ...
Ten Overlooked Issues in the IPCC and US National Assessments
Ten Overlooked Issues in the IPCC and US National Assessments

Haydn Washington – Climate Change Denial
Haydn Washington – Climate Change Denial

... Celsius (well within previous natural temperature variations) occurred between 1979 and 1998, and has been followed by slight global cooling over the past 10 years.” Bob Carter ...
Features
Features

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Global warming hiatus



A global warming hiatus, also sometimes referred to as a global warming pause or a global warming slowdown, is a period of relatively little change in globally averaged surface temperatures. In the current episode of global warming many such periods are evident in the surface temperature record, along with robust evidence of the long term warming trend.The exceptionally warm El Niño year of 1998 was an outlier from the continuing temperature trend, and so gave the appearance of a hiatus: by January 2006 assertions had been made that this showed that global warming had stopped. A 2009 study showed that decades without warming were not exceptional, and in 2011 a study showed that if allowances were made for known variability, the rising temperature trend continued unabated. There was increased public interest in 2013 in the run-up to publication of the IPCC Fifth Assessment Report, and despite concerns that a 15-year period was too short to determine a meaningful trend, the IPCC included a section on a hiatus, which it defined as a much smaller increasing linear trend over the 15 years from 1998 to 2012, than over the 60 years from 1951 to 2012. Various studies examined possible causes of the short term slowdown. Even though the overall climate system had continued to accumulate energy due to Earth's positive energy budget, the available temperature readings at the earth's surface indicated slower rates of increase in surface warming than in the prior decade. Since measurements at the top of the atmosphere show that Earth is receiving more energy than it is radiating back into space, the retained energy should be producing warming in at least one of the five parts of Earth's climate system.A July 2015 paper on the updated NOAA dataset cast doubt on the existence of this supposed hiatus, and found no indication of a slowdown. This analysis incorporated the latest corrections for known biases in ocean temperature measurements, and new land temperature data. Scientists working on other datasets welcomed this study, though the view was expressed that the short term warming trend had been slower than in previous periods of the same length.
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